On the magnet, magnetick bodies also, and on the great magnet the earth: a new physiology, demonstrated by many arguments & experiments
History
On the magnet, magnetick bodies also, and on the great magnet the earth: a new physiology, demonstrated by many arguments & experiments
Magnetism -- Early works to 1800
Why Iron touched by a Loadstone acquires an opposite
_verticity, and why iron touched by the true Northern side of a stone_
turns to the North of the earth, by the true Southern side
_to the South; and does not turn to the South when rubbed
by the Northern point of the stone, and when by
the Southern to the North, as all who have
written on the loadstone have
falsely supposed._
Demonstration has already been given that the northern part of a loadstone
does not attract the northern part of another stone, but the southern, and
repels the northern part of another stone from its northern side when it is
applied[203] to it. That general magnet, the terrestrial globe, disposes
iron touched by a loadstone in the same way, and likewise magnetick iron
stirs this same iron by its implanted strength, and excites motion and
controls it. For whether the comparison and experiment has been made
between loadstone and loadstone, or loadstone and iron, or iron and iron,
or the earth and loadstone, or the earth and iron conformed * by the earth
or strengthened by the power of a loadstone, the strength and inclinations
of each must mutually harmonize and accord in the same way. But the reason
must be sought, why a piece of iron when touched by a loadstone acquires a
disposition to motion toward the opposite pole of the earth, and not toward
that {126} pole of the earth to which that pole of that loadstone turned by
which it was excited. It has been pointed out that iron and loadstone are
of one primary nature; when the iron is joined to the loadstone, they
become, as it were, one body, and not only is the end of the iron changed,
but the remaining parts also are affected along with it. A, the north pole
of a loadstone, is placed against the cusp of a piece of iron; the cusp of
the iron has now become the southern part of the iron, [Illustration]
because it is touching the northern part of the stone; the cross-end of the
iron has become the northern. For if that contiguous magnetick substance be
separated from the pole of the terrella, or from the parts near the pole,
the one end (or the end which, whilst the connection was kept up, was
touching the northern part of the stone) is the southern, whilst the other
is the northern. So also if a versorium excited by a loadstone be divided
into ever so many parts (however small), those parts when separated will,
it is clear, arrange themselves in the same disposition as that in which
they were disposed before, when they were undivided. Wherefore whilst the
cusp remains over the northern pole A, it is not the southern end, but is,
as it were, part of a whole; but when it is taken away from the stone, it
is the southern end, because when rubbed it tended toward the northern
parts of the stone, and the cross (the other end of the versorium) is the
northern end. The loadstone and the iron make one body; B is the south pole
of the whole; C (that is, the cross) is the northern end of the whole;
Public-domain text, read in full here on John Shaqi.
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